亜氷河のボストーク湖と,その上に覆われている氷床の間の水交換
1Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, UK. m.j.siegert@bristol.ac.uk
Nature
|February 25, 2000
まとめ
ウォストーク湖の氷床下の融解と凍結は,氷床と湖の間の重要な水交換を示しています. このプロセスは氷河下の環境に影響を与え,生命を支える可能性がある.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- 氷河学 氷河学とは
- 天体生物学 アストロバイオロジー
背景:
- ヴォストーク湖は,南極の200kmの氷河下の湖で,ヴォストーク駅の氷床の下にあります.
- 氷床の底部の条件は,亜氷河湖の環境と潜在的な居住可能性についての洞察を提供します.
研究 の 目的:
- 空中レーダーを使用して,ヴォストーク湖上の氷床構造を分析する.
- 氷床下湖のインターフェイスにおける氷水相互作用のダイナミクスを理解するために.
主な方法:
- 氷床の構造を研究するために,空中60MHzレーダー調査が行われました.
- 分析は,基礎氷の減少と蓄積のゾーンを特定することに焦点を当てました.
主要な成果:
- 氷と水の界面で,基礎氷の減少と蓄積の明確なゾーンが特定されました.
- サブ氷河の融解と氷の損失は,湖の北側と西側で起こります.
- 約150mの氷の蓄積 (凍結) が湖の南側で発生しています.
結論:
- 氷床の底部とヴォストーク湖の間に,重要な水の交換が起こります.
- この交換は湖をガス水素で豊かにし,堆積物の堆積を促進し,湖水循環を推進する.
- この発見は,亜氷河環境の居住可能性を理解するための意味を持つ.
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